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received water from groundwater sources. Along the 110 potential bottomland sites, we estimated 13.4 miles (21.6 km) of natural levees and 26.6 miles (42.9 km) of human-made dikes and levees. Of the various bottomland habitat types, 41 were floodplain terraces, 23 gravel-pit ponds, 22 side channels, and 16 canyon mouths. The remaining flooded habitat types consisted of 13 floodplain depressions and one oxbow. All 13 depressions were located between Moab Slough and the Green River confluence. Three of these depression habitat sites (rm 50.9-52.5 [rkm 82- 84], rm 33.2-35.6 [rkm 53-57], and rm 17.5-18.7 [rkm 28-30]), may be important off-channel habitats for razorback sucker drifting downstream if an expected or planned upstream spawning area is identified. Although these areas are wet during high water, they appear isolated from the river in photos and water enters only by groundwater infiltration and, therefore, fish do not have access to these areas. Further on-ground investigation of these areas is needed to determine water depth during runoff to monitor water duration, and to evaluate if fish can access these areas during high water. Gunnison River. There were 48 bottomland habitat sites with a potential (historical) of 3,227 acres (1,306 ha) along the Gunnison River (rm 0-75 [rkm 0-121]) in 1993 (Appendix D; Table D.2.). Of this total, 828 acres (335 ha; 41 sites) were inundated during the May and June high water period and 161 acres (459 ha) in the September low-water flow period. In the Gunnison River, there was only one general area where bottomland habitats were concentrated. This was in the 17-mile stream reach in the Delta, Colorado, area that extends from Roubideau Creek upstream to Austin (rm 50-67 [rkm 81-108]). There were 1,739 acres (705 ha) of potential floodplain habitat in this 17-mile reach. The remaining 50 miles of warmwater stream reach downstream of Roubideau Creek can be predominantly classified as canyon- bound with few bottomland habitat sites. Eighty-five percent of the 41 sites flooded in May had a hydrological connection to the river, whereas 76% (13 sites) of the 17 sites still wet in September were connected to the-river (Appendix E; Tables E.14 to E.16.). Although 41 of 48 sites were inundated during May and June, only 17 sites had one surface connection to the river and 16 sites had both and up- and downstream surface connection. Thirteen of the May flooded sites received some water from a gravity-fed (irrigation) water source. Along the 48 potential bottomland sites, we estimated 1.2 miles (2 km) of natural levees and 8.3 miles (13.4 km) of human-made dikes and levees. Of the various bottomland habitat types, 35 were floodplain terraces, six gravel- pit ponds, three oxbows, and two side channels. The remaining habitat types consisted of one floodplain depression and one canyon mouth. Site Scoring and Prioritization All bottomland habitat sites identified, 135 in the Green River Drainage (Appendix F; Table F.1.) and 158 in the Colorado River drainage (Appendix F; 20